Academic literature on the topic 'Area drenata'

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Journal articles on the topic "Area drenata"

1

Cień, Damian, Jacek Motyka, and Kajetan d’Obyrn. "Zmiany natężenia przepływu w rzece Sztole (rejon olkuski) w warunkach drenażu górniczego." Przegląd Geologiczny 70, no. 10 (2022): 761–69. http://dx.doi.org/10.7306/2022.29.

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Stoyan Vergiev. "Detailed GIS mapping of communities of plants with conservation status and defining the touristic zones in the group "Kanarata and Quarry Drenaka" of the protected area "Pobiti Kamani" (Northeastern Bulgaria)." GSC Biological and Pharmaceutical Sciences 16, no. 3 (2021): 085–90. http://dx.doi.org/10.30574/gscbps.2021.16.3.0269.

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The aims of the present study were: 1) to perform a detailed mapping of the distribution of conservationally significant (endemic, vulnerable, endangered and protected) plant species in the group "Kanarata and Quarry Drenaka" of the protected area "Pobiti Kamani" for 2020 yr in GIS environment; 2) based on the overlap of the distribution sites of plant species, to determine the "hot spots" of plant biodiversity, access to which should be limited in order to protect them and at the same time to identify areas with no or low concentration of conservationally important species in order to trace and mark the tourist paths in the protected area. In order to investigate the distribution of six plant communities, a detailed GIS mapping was performed. As a result of the study, detailed distribution maps of investigated species communities in Central Group were drawn. Special attention is paid to the zones where two or more communities were overlapped. The identification of the areas with concentration of conservation-significant species and localization of "hot spots" is crucial for protection management of the group "Kanarata and Quarry Drenaka" of the protected area "Pobiti Kamani". The model of "hot spots" and the model of overlapping are applicable and in combination with detailed distribution maps are fundamental for more successful protection and conservation. The suggested touristic zones with lack of conservation species can be used to trace and to construct environmentally friendly tourist trail and paths without destroying and harming the species, their habitats, and the aesthetic and recreational value of the landscapes.
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BYTYQI, Valbon Xh. "THE IMPACTS OF SETTLEMENT EXTENSION ON SOIL RESOURCES: A CASE STUDY IN DRENICA RIVER BASIN (KOSOVO)." Media Komunikasi Geografi 19, no. 1 (2018): 101. http://dx.doi.org/10.23887/mkg.v19i1.13951.

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Rapid extension of settlements in Kosovo has made major changes in land use and land cover. Migration of population towards plains has reduced the number of inhabitants in hilly-mountainous areas where low fertile soils are found. Significant part of agricultural land are changed from primary destination, and agricultural potentials are reduced. Urbanization in many cases is made in unplanned way, and in our study area in Drenica River basin are observed land degradation forms and other environmental transformations where in some cases the risk of flooding increased and floods appeared. This study about Drenica River basin will discuss aspects of the influence of morphology, water flows, and the land capability in the distribution of population, and will be a contribution to sustainable urbanization of settlements and agricultural land preservation. In order to accomplish the research are used satellite images, maps of different years, and the census data for the purpose of better coverage that has influence in the process of urbanization on soil resources in Drenica River basin (Kosovo).
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Depettris, Carlos A., Jorge V. Pilar, Hugo R. Rohrmann, and Marcelo J. M. Gómez. "Análisis de precipitaciones extremas en el área metropolitana del Gran Resistencia." Aqua-LAC 13, no. 1 (2021): 1–15. http://dx.doi.org/10.29104/phi-aqualac/2021-v13-1-01.

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En el año 2019, el Área Metropolitana del Gran Resistencia, conformada por las localidades de Resistencia, Barranqueras, Puerto Vilelas y Fontana, ha soportado precipitaciones extremas durante los meses de enero y abril, cuyas consecuencias fueron inundaciones en numerosos barrios del casco céntrico y de las áreas periféricas, con el consecuente deterioro de la infraestructura urbana y problemas ambientales como la diseminación incontrolada de basura con un colapso del sistema de conducción de líquidos cloacales. La ocurrencia de estos eventos extremos diarios, medidos en la Estación Campus Resistencia de la UNNE, han sido producto de un calentamiento extraordinario de la atmósfera en la región central de Sudamérica desde abril de 2018, un debilitamiento de los sistemas frontales de la región antártica y un sostenimiento del calentamiento superficial del Océano Atlántico, creándose un corredor libre de concentración de humedad en la región. Dadas las condiciones críticas que para la población y la infraestructura se generan en el AMGR ante la ocurrencia de los eventos mencionados, se consideró necesario realizar una estimación de la Precipitación Máxima Probable (PMP) para una duración diaria aplicando el criterio estadístico de Hershfield, lo que arrojó un valor para el Factor de Frecuencia Φ = 5, resultando como consecuencia una PMP diaria de 302.2 mm, monto que debería ser tenido en cuenta para llevar adelante el diseño de los planes de contingencia a incluir en un Plan Director de Drenaje Urbano que aún falta desarrollar para esta región.
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Kutllovci, Festim, and Islam Fejza. "Petrographic characteristics in the central part of Kosovo." Mining of Mineral Deposits 15, no. 4 (2021): 139–44. http://dx.doi.org/10.33271/mining15.04.139.

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Purpose. This paper aims to provide complete identification of rock types in the Drenas region by detailed description of all types of the rocks found. The authors intended to determine interruption or continuity of all inter-formational boundaries to accurately delineate them on the ground and fully reflect on the 1: 25000 scale map, as well as to identify the nature of contact between rock types and give its detailed description. Methods. During August, September, October of 2019, the exploration field trips were carried out. Geological survey works focused on the following areas: complete identification of all rock types on the basis of studying their samples, preparation of thin sections for petrographic (only the magmatic rock), chemical and geochemical analysis. Systematic measurement of structural elements was conducted alongside with identification and description of mineral outcrops areas. Findings. Based on the study of stratigraphic units and geological description of mineral outcrop areas, we identified different types of rocks using petrography microscope preparation and chemical and geochemical analysis. The area of Drenas has the following lithostratigraphic units: gabbro diabase, harzburgite, metasandstone. Originality. The originality of the study consists in the use of optical microscope for precise identification of rocks. As a result of the research conducted in the exploration area, we have obtained a clear petrographic description of minerals composition, their texture and mineralization, which allows assessing the possibility of the area exploitation. The analyses were completed at the certified laboratory of Geology-Mining Faculty (Polytechnic University of Tirana) and Geosciences Institute. Practical implications. Petrographic study and chemical analysis led to the conclusion that the research area has Ni mineralization, which is important for the development of mining sector and the community given the environment is preserved and the adequate way of the area exploitation is applied.
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Gonçalves, Gustavo Leite, Francimagne Ribeiro da Silva, Maria Rosimery de Carvalho, Sarah de Souza Cruz Mendonça, and Joel Medeiros Bezerra. "ZONEAMENTO AMBIENTAL DA MICROBACIA HIDROGRÁFICA DO AÇUDE DA CACHOEIRA – CEARÁ, BRASIL." InterEspaço: Revista de Geografia e Interdisciplinaridade 5, no. 19 (2020): 202014. http://dx.doi.org/10.18764/2446-6549.e202014.

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ENVIRONMENTAL ZONING OF MICRO WATERSHED AÇUDE DA CACHOEIRA – CEARÁ, BRAZILZONIFICACIÓN AMBIENTAL DE LA MICRO CUENCA HIDROGRÁFICA DEL AÇUDE DA CACHOEIRA – CEARÁ, BRASILRESUMOA bacia hidrográfica, considerada como um conjunto de terras drenadas por um corpo d’água principal e seus afluentes, representa a unidade mais apropriada para o estudo qualitativo e quantitativo dos recursos hídricos, sendo uma unidade ambiental que possibilita tratar dos componentes e da dinâmica das inter-relações necessárias ao planejamento e à gestão ambiental. Os impactos de degradação em bacias hidrográficas são advindos dos múltiplos usos, má gestão e ações antrópicas, sendo necessários o controle e a regulação de ocupação do solo visando à manutenção da qualidade, quantidade e regularidade da água para seus diversos usos. Dessa forma, o presente estudo teve por objetivo realizar a delimitação da Microbacia Açude da Cachoeira – MAC, localizada em maior parte no município de Aurora, estado do Ceará, bem como identificar e discutir dados gerais sobre a rede de drenagem, os parâmetros morfométricos, carta temática hidrográfica, relevo e Áreas de Preservação Permanente – APP’s. Os dados foram obtidos por meio do software gratuito QGIS com auxílio da ferramenta Google Earth Pro para a determinação da microbacia e rede de drenagem, além da delimitação das APP’s dos corpos hídricos e análise das potencialidades. Como resultados, constatou-se que a rede de drenagem da MAC apresenta baixa distribuição do escoamento, no qual oferece um menor risco a enchentes em picos de intensidades chuvosas. Além disso, seus canais de drenagem dispõem de um ordenamento hídrico de quarta ordem e seu escoamento global a classifica como uma bacia endorreica.Palavras-chave: Análise Morfométrica; Rede de Drenagem; Semiárido Brasileiro.ABSTRACTThe watershed, considered as a set of lands drained by a main body of water and its tributaries, represents the most appropriate unit for the qualitative and quantitative study of water resources, being an environmental unit that allows to treat the components and use the necessary interrelationships for environmental planning and management. The impacts of degradation in watersheds are the result of multiple uses, mismanagement and anthropic actions, requiring the control and regulation of land occupation in order to maintain the quality, quantity and regularity of water for its various uses. Thus, the present study aimed to delineate the Açude da Cachoeira watershed - ACMW, located mostly in the municipality of Aurora, Ceará state, as well as to identify and discuss general data about the drainage network, the morphometric parameters, hydrographic thematic chart, relief and Permanent Preservation Areas – PPA’s. The data were obtained through the free software QGIS with the aid of the Google Earth Pro tool for the determination of the micro watershed and drainage network, as well as the delimitation of water bodies PPA’s and potentiality analysis. As a result, it was found that the ACMW drainage network has low runoff distribution, which offers a lower risk of flooding at rainy peak. In addition, its drainage channels have a fourth order water structure and its global flow classifies it as an endorheic basin.Keywords: Morphometric Analysis; Drainage Network; Brazilian Semiarid.RESUMENLa cuenca hidrográfica, considerada como un conjunto de tierras drenadas por un cuerpo principal de agua y sus afluentes, representa la unidad más apropiada para el estudio cualitativo y cuantitativo de los recursos hídricos, siendo una unidad ambiental que permite tratar dos componentes de las interrelaciones dinámicas necesarias para la planificación y gestión ambiental. Los impactos de la degradación en las cuencas hidrográficas son el resultado de múltiples usos, mala gestión y acciones antrópicas, que requieren el control y la regulación de la ocupación de la tierra para mantener la calidad, cantidad y regularidad del agua para sus diversos usos. Por lo tanto, el presente estudio tuvo como objetivo delinear la micro cuenca hidrográfica del Açude da cachoeira- MHAC, ubicada principalmente en el municipio de Aurora, estado de Ceará, así como identificar y discutir datos generales sobre la red de drenaje, los parámetros morfométricos, carta temática hidrográfica, relieve y áreas de preservación permanente - APP's. Los datos se obtuvieron a través del software gratuito QGIS con la ayuda de la herramienta Google Earth Pro para la determinación de la red de micro cuencas y drenaje, además de la delimitación de las aplicaciones de los cuerpos de agua y el análisis de las potencialidades. Como resultado, se descubrió que la red de drenaje MHAC tiene una baja distribución de escorrentía, lo que ofrece un menor riesgo de inundación en el pico lluvioso. Además, sus canales de drenaje tienen un ordenamiento hidrico de cuarto orden y su flujo global lo clasifica como una microcuenca endorreica.Palabras clave: Análisis Morfométrico; Red de Drenaje; Semiárido Brasileño.
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7

Fejza, Islam, Astrit Shala, Festim Kutllovci, and Ahmet Tmava. "Petrographic and geochemical characteristics of rocks in the Drenas region, Kosovo." Mining of Mineral Deposits 16, no. 2 (2022): 110–15. http://dx.doi.org/10.33271/mining16.02.110.

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Purpose. The paper purpose is to provide complete identification of rock types and the geochemical characteristics in the Drenas region. The authors seek to determine the discontinuity or continuity of all inter-formational boundaries to accurately delineate them in the field and fully reflect on a 1:25000 scale map. In addition, they reveal the nature of the contact between rock types, giving its detailed description and geochemical characteristics. Methods. Geological study is focused on the following facts: complete identification of all rock types on the basis of studying their samples, preparation of thin sections for petrographic study, chemical and geochemical analysis. The methods applied for geochemical analysis use the MinPet software. This software, used for mineral chemistry, is programmed to process and recalculate the results of major-element analysis according to the most common normative calculation schemes. This software is used in scientific works for constructing diagrams of rock calcification and geochemical interpretations according to the components of Na2O + K2O/SiO2, as well as rare earth elements according to the component SiO2/Zr/TiO2. The exploration field trips have been conducted to identify and describe areas of mineral outcrop. Findings. Based on the study of geochemical analysis and the petrographic description of mineral outcrops, as well as examination under a microscope, different types of rocks have been identified. Based on these types, the origin, age and spread of these rocks in this region have been determined. Originality. The originality of the study is in the use of the analysis results obtained in the AcmelLabs Laboratory, Vancouver, Canada, for major elements, rare earth elements and trace elements, which are shown in the diagrams presented in this paper. Practical implications. The geochemical analysis leads to the conclusion that the studied area has Ni-mineralization, which is important for the development of mining sector, as well as for the community while preserving the environment and applying an adequate method of exploiting the area.
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8

Palomeque-De la Cruz, Miguel Á., Adalberto Galindo-Alcántara, Miguel J. Escalona-Maurice, Silvia del C. Ruiz-Acosta, Alberto J. Sánchez-Martínez, and Eunice Pérez-Sánchez. "Analysis of land use change in an urban ecosystem in the drainage area of the Grijalva river, Mexico." Revista Chapingo Serie Ciencias Forestales y del Ambiente 23, no. 1 (2016): 105–20. http://dx.doi.org/10.5154/r.rchscfa.2016.03.018.

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9

Krasniqi, Elez, and Fadil Millaku. "The Association Hyperico-Euphorbietum Glabriflorae Rexhepi 1978 in the Serpentine Terrains of Drenica Mountain." Hacquetia 6, no. 2 (2007): 183–93. http://dx.doi.org/10.2478/v10028-007-0008-6.

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The AssociationHyperico-Euphorbietum GlabrifloraeRexhepi 1978 in the Serpentine Terrains of Drenica MountainIn the territory of Kosovo there are many serpentine mountain massifs. The largest complexes are found in the valley of the Ibër River, and the same are continued in a discontinuous chain through Koznica and Golesh to the southwest of the territory of Kosovo. Vegetation on the serpentine bedrock is rich in rare species and communities, which cannot be found in the Balkans and Europe. The communities appearing on the serpentine bedrock are characteristic and important for science. They are endemic due to the presence of endemic species in their species composition. Drenica Mountain (1051 m) is part of the Central Kosovo Mountains. These terrains are situated in the central part of Kosovo, between Çiçavica, Kosovo plain (Golesh), Llapusha, the Carraleva Mountains and the Anadrini region. A considerable part of these areas consists of serpentine bedrock, which is covered by interesting flora and vegetation. In the vegetation of Drenica Mountain 10 communities have been identified. Two of them are found on serpentine bedrock: ass.Hyperico-Euphorbietum glabrifloraeand ass.Potentillo-Fumanetum bonapartei. These communities belong to the open space, and are also located in other parts of Kosovo, but only on serpentine bedrock. On Drenica Mountain there are two localities where these two communities appear. In this paper we focus in particular on ass.Hyperico-Euphorbietum glabriflorae
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Fernandes, Manoel Do Couto, André De Souza Avelar, and Ana Luiza Coelho Netto. "Domínios geo-hidroecológicos do maciço da Tijuca, RJ: subsídios ao entendimento dos processos hidrológicos e erosivos." Anuário do Instituto de Geociências 29, no. 2 (2006): 122–48. http://dx.doi.org/10.11137/2006_2_122-148.

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Tijuca massif constitute a geomorphologic system, where the replacement of vegetation cover by urban features and grass areas, contribute to change in the hydrological behavior.As a consequence of this change there is an increase of erosion processes by different mechanisms, and in the solid and liquid discharge that can affect lowlands. The understanding of these processes, in a geoecological research above center of interest geomorphologic view requires the interpretation of the elements control them, in structural, functional and dynamic way. This way, the aim at interpreting the transformation processes that occur in this massif, and delimitate the use and covering of the soil that with others structural and functional elements define areas with differents hydrological and erosive results (geo-hydroecological dominions). To define this dominions, it was taken into consideration systematically, the soil use, type and characteristic of the soil, geology and drenage efficiency, using geoprocessing technic and analytic-integrative method. The results show that in the sectors 1, 2 and 5 have dominions that make is inundation in them lowlands. The areas of urbarn ocupation in the sectors 2, 3 e 4 concentrate the landslides, because in this areas occur the bigger drenage efficiency, reflex of higher gradients and density of concave axis. In this way the continuatily will promote a drastic growth of Tijuca massif's erosive processes.
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